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GETTING STARTED
Installation
Where to Run Things?
Python Packages
Mondaic Downloader
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Example Site Configurations
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Knowledge Base
Wave Equation
Boundary Conditions
Natural Boundary Conditions
Homogeneous Dirichlet
Absorbing Boundaries
Mesh Generation
Spectral-Element Modelling
Dispersion Error
Wavefield Separation
Parameterizations
Units
Inverse Problems
Velocity Misfits
Gradient Misfits
Examples & Tutorials
Tutorials
Getting started
Part 1 - First simulation
Part 2 - Verification
Part 3 - Visualization
Part 4 - Heterogeneous models
Models and topography
1D models
Model order
Parameterizations
Simple topography
Layered models
Heterogeneous models and slice extraction
Marmousi
3D surface topography
Meshing
Importing external meshes
Mesh-to-mesh interpolation
Cylindrical meshes
Data-adaptive mesh masking
Goal-oriented meshing with SmoothieSEM
Sources and receivers
Introduction
Locating sources and receivers
Custom source time functions
Equivalence of filtering STFs and filtering synthetics
Waveform physics
Attenuation
Acoustic VTI
2D teleseismic simulation
Ocean loading
Data analysis
Receiver Gathers
Wavefield Output
Inversion
Full-waveform inversion
Part 1 - Setup
Part 2 - Synthetics
Part 3 - Sensitivities
Part 4 - Iterations
Part 5 - Extensions
Gradient preconditioning
Smoothing
Homogeneous media
Gradients for Seismology
Advanced Interface
Lamb's problem
Model interpolation
SalvusFlow API
Manual gradient computation
Marmousi
Applications
Seismology
Continental-scale simulations
Sensitivity kernels
Global-scale simulation
Geotech
Ground motion modeling of buildings
Real data continental-scale FWI
Part 0 - Prologue
Part 1 - Project setup & data acquisition
Part 2 - Forward simulations
Part 3 - Data selection and misfit definition
Part 4 - Iterative inversion
Near Surface
Part 0 - Prologue
Part 1 - Project setup & importing external data
Part 2 - Starting Model
Part 3 - 3D-to-2D Conversion
Integration Tests
Analytic Tests
Semi-analytic test - Acoustic
Semi-analytic test - Elastic
Semi-analytic test - Coupled
On-the-fly Fourier transform
Analytic test - Diffusion equation
Analytic test - Poisson's equation
Gradient Tests
Gradient test simple physics
Gradient test TTI medium
Reference Documentation
SalvusCompute API
SalvusMesh Interfaces
AxiSEM
AxiSEMCartesian
Cartesian2D
Cartesian3D
Cartesian2DHomogeneous
Cartesian3DHomogeneous
Circular2D
Globe3D
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SmoothieSEM
SphericalChunk3D
SphericalChunk3DSurfaceWaves
TidalLoading
Python API
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fem
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data_proxies
seis_io_data_proxy
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segy_data_backend
xarray_data_backend
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event_data
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types
event_window_and_weight_set
wavefield_compression
paths
api
simple_config
receiver
seismology
collections
cartesian
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simulation
boundary
source
transformations
cartesian
collections
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stf
sites
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lsf
pbs
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ssh
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run_task_chain_bash_file
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task_chain_controller
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mesh_from_domain
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layered_model
bm
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layer
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layered_model
material
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isotropic
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dim3
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isotropic
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visco
acoustic
elastic
parameter
meshing_protocol
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detail
interlayer_constant
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interlayer_doubling
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meshing_protocol
interface
detail
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curve
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utils
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attenuation
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mask_generators
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simple_mesh
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unstructured_mesh_utils
modules
near_surface
processing
point_to_line_source_conversion
geophone_response
source_inversion
source_inversion
waveform_db
utils
waveform_db
namespace
opt
mappings
mappings
methods
lbfgs
trustregion
iteration
misfits
cross_correlation_time_shift
gradient_test
deprecated
phase_misfit
graph_space_optimal_transport
l2_misfit
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failed_result
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generate_cleanup_task
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meshing
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PUBLICATIONS
python_api
/
salvus
/
mesh
/
models_1D
salvus.mesh.models_1D
A class to handle 1D seismic velocity models
Functions
str2bool()
Classes
ConstInterpolator
model
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basic_mesh
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unstructured_mesh
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